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    华北盆地梁村古潜山岩溶热储聚热机制及资源潜力

    康凤新 赵季初 黄迅 隋海波

    康凤新, 赵季初, 黄迅, 隋海波, 2023. 华北盆地梁村古潜山岩溶热储聚热机制及资源潜力. 地球科学, 48(3): 1080-1092. doi: 10.3799/dqkx.2022.324
    引用本文: 康凤新, 赵季初, 黄迅, 隋海波, 2023. 华北盆地梁村古潜山岩溶热储聚热机制及资源潜力. 地球科学, 48(3): 1080-1092. doi: 10.3799/dqkx.2022.324
    Kang Fengxin, Zhao Jichu, Huang Xun, Sui Haibo, 2023. Heat Accumulation Mechanism and Resources Potential of the Karst Geothermal Reservoir in Liangcun Buried Uplift of Linqing Depression. Earth Science, 48(3): 1080-1092. doi: 10.3799/dqkx.2022.324
    Citation: Kang Fengxin, Zhao Jichu, Huang Xun, Sui Haibo, 2023. Heat Accumulation Mechanism and Resources Potential of the Karst Geothermal Reservoir in Liangcun Buried Uplift of Linqing Depression. Earth Science, 48(3): 1080-1092. doi: 10.3799/dqkx.2022.324

    华北盆地梁村古潜山岩溶热储聚热机制及资源潜力

    doi: 10.3799/dqkx.2022.324
    基金项目: 

    国家自然科学基金项目 U1906209

    国家自然科学基金项目 42072331

    详细信息
      作者简介:

      康凤新(1968—),男,研究员,博士,主要从事水文地质地热地质研究. ORCID:0000-0002-3615-8729. E-mail:kangfengxin@126.com

      通讯作者:

      赵季初, ORCID: 0000-0002-3346-9425. E-mail: 597943119@qq.com

    • 中图分类号: P314

    Heat Accumulation Mechanism and Resources Potential of the Karst Geothermal Reservoir in Liangcun Buried Uplift of Linqing Depression

    • 摘要: 地热是一种绿色低碳的清洁能源,其规模化开发利用对减少碳排放量与改善大气环境意义重大,为促进中低温水热型地热流体发电技术在实现“双碳”目标中的应用,本文在揭示梁村古潜山潜凸起岩溶热储聚热机制、评价资源潜力的基础上,对10 MW地热电站示范工程的资源保证能力进行了论证.通过地温梯度、大地热流值与构造格架、岩石热导率相关性对比分析,岩溶发育特征、热储富水性与构造、岩性、水动力条件组合关系研究,揭示了梁村古潜山潜凸起岩溶热储的四元聚热机制:一元为华北克拉通破坏、岩石圈减薄导致的高大地热流传导聚热,二元为凸起区高热导率分流聚热,三元为深大断裂带对流聚热,四元为成岩压密水对流聚热;计算出梁村古潜山潜凸起寒武系-奥陶系裂隙岩溶热储中蕴藏的可利用热资源量为2.218 3×1019 J、地热水资源量为6.34×109 m3.在四元聚热驱动下,形成了梁村古潜山潜凸起高地温梯度岩溶热储地热田,其热能量与地热流体资源量满足10 MW地热电站建设需求.

       

    • 图  1  研究区地质构造略图

      Fig.  1.  Sketch of tectonic structure at study area

      图  2  研究区地层剖面

      Fig.  2.  Stratigraphic profile at study area

      图  3  研究区奥陶系顶埋深等值线

      Fig.  3.  Contour map of burial depth of Ordovician in the study area

      图  4  华北克拉通破坏与东部减薄的地壳(33 km)和岩石圈(60~100 km)

      据Zhu and Cheung(2012)、Kusky et al.2014)修改

      Fig.  4.  The destruction of North China Craton and eastern thinned crust (33 km) and lithosphere (60~100 km)

      图  5  临清坳陷梁村古潜山潜凸起岩溶热储聚热机制模式

      Fig.  5.  Conceptual model of Liangcun uplift karst geothermal reservoir

      图  6  计算区划分简图

      Fig.  6.  Zonation map for geothermal resource estimation

      表  1  我国曾建中低温水热型地热电站

      Table  1.   Past geothermal power plant of mid-low temperature water type geothermal resource

      地点 温度(℃) 装机容量(kW)
      广东丰顺县邓屋 92 300
      湖南宁乡县灰汤 98 300
      河北怀来县后郝窑 87 200
      山东招远县汤东泉 98 300
      辽宁盖县熊岳 90 200
      广西象州市热水村 79 200
      江西宜春县温汤 67 100
      下载: 导出CSV

      表  2  梁古1孔寒武纪‒奥陶纪地层特征

      Table  2.   Lithological properties of Cambrian-Ordovician strata unveiled in Lianggu1 borehole

      地层划分 埋深(m) 层厚(m) 岩性
      层顶 层底
      八陡组 3 340 3 345 5 薄层泥晶灰岩与白云岩互层
      3 345 3 350 5 中厚层泥晶灰岩
      3 350 3 355 5 中厚层白云岩
      3 355 3 378 23 中厚层泥晶灰岩夹薄层泥灰岩
      3 378 3 401 23 中厚层泥晶灰岩
      3 401 3 420 19 薄层泥晶灰岩与泥灰岩互层
      3 420 3 475 55 中厚层泥晶灰岩
      阁庄组 3 475 3 550 75 中厚层白云岩夹泥晶灰岩
      3 550 3 572 22 中厚层泥晶灰岩
      3 572 3 584 12 薄层泥质白云岩、泥灰岩夹白云岩
      五阳山 3 584 3 642 58 中厚层泥晶灰岩
      3 642 3 687 45 中厚层泥晶灰岩与薄层泥灰岩互层
      3 687 3 817 130 中厚层泥晶灰岩
      3 817 3 829 12 薄层白云岩,夹泥晶灰岩、泥灰岩
      3 829 3 875 46 中厚层泥晶灰岩,夹薄层泥灰岩、白云岩
      3 875 3 887 12 薄层白云岩
      3 887 3 917 30 中厚层泥晶灰岩,夹薄层白云岩
      3 917 3 927 10 薄层白云岩,夹泥晶灰岩、泥质白云岩
      3 927 3 975 48 中厚层泥晶灰岩,夹薄层白云岩
      土峪组 3 975 4 010 35 中厚层白云岩
      4 010 4 027 17 中厚层泥灰岩
      4 027 4 043 16 中厚层泥晶灰岩
      4 043 4 058 15 薄层泥灰岩
      北庵庄组 4 058 4 080 22 中厚层泥晶灰岩
      4 080 4 091 11 中厚层白云岩
      4 091 4 151 60 中厚层泥晶灰岩,夹薄层白云岩
      东黄山组 4 151 4 171 20 中厚层泥质白云岩
      4 171 4 179 8 中厚层泥晶岩
      4 179 4 186 7 中厚层泥灰岩
      下载: 导出CSV

      表  3  热储可利用热资源量计算值

      Table  3.   Geothermal resource estimation table

      分区 面积(km2) 顶板埋深(m) 温度(℃) 地热水密度(kg/m3) 热资源量(J) 5 ℃温差热资源量(J) 地热水资源量(m3)
      96.98 4 000~5 000 150 916.8 1.157 4×1019 8.267 2×1017 2.93×109
      51.97 3 500~4 000 135 930.3 4.878 1×1018 4.434 7×1017 1.57×109
      61.05 3 000~3 500 135 930.3 5.730 4×1018 5.209 5×1017 1.84×109
      合计 210 2.218 3×1019 1.791 1×1018 6.34×109
      下载: 导出CSV

      表  4  不同发电工质下地热水单位流量净发电量

      Table  4.   Net power generation capacity of geothermal water for different working fluid

      地热井口温度(℃) 发电量(kW·h/t)
      R123a R600a R152a
      80 1.29 1.34 1.29
      90 1.9 2.12 2.02
      100 2.75 2.89 2.75
      110 3.59 3.99 3.8
      120 4.77 5.09 4.84
      130 5.92 6.57 6.28
      140 7.4 8.05 7.72
      150 8.91 9.99 9.69
      160 10.69 11.92 11.65
      170 12.54 14.44 14.47
      180 14.74 16.95 17.29
      注:据马峰等(2021).
      下载: 导出CSV

      表  5  不同发电工质、地热井口温度条件下所需地热水资源量

      Table  5.   The amount of geothermal water resources required under the conditions of different generating working quality and geothermal water temperature

      地热井口温度(℃) R123a(m3 R600a(m3 R152a(m3
      130 4.44×108 4.00×108 4.18×108
      140 3.55×108 3.26×108 3.40×108
      150 2.95×108 2.63×108 2.71×108
      下载: 导出CSV
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    • 收稿日期:  2022-08-05
    • 网络出版日期:  2023-03-27
    • 刊出日期:  2023-03-25

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